During the last decade, severe winters were frequently observed over mid-latitude Eurasia, despite continuous increase in greenhouse gas concentrations. Statistical analysis of observation have suggested that these cold Eurasian winters were excited by Arctic sea-ice decline. However, it is not yet clear whether the cooling anomalies are a dynamical response to the sea-ice loss or natural fluctuation of the atmosphere, because a robust response is yet to be obtained in the numerical model simulations due to energetic internal fluctuations in the atmospheric circulation. In this research, we successfully detected the signature of Eurasian cold winters excited by sea-ice decline in the Barents-Kara Sea (BKS), by generating a 100-member ensemble of state-of-the-art atmospheric general circulation model simulations driven with realistic sea-ice concentration anomalies. We will conclude that the observed cold Eurasian winters in the previous decade are attributable to a combination of the natural fluctuation and the response to sea-ice loss, the latter having larger contributions.